ATLANTIC ATOC NETWORK DESIGN STUDIES
Principal Investigator:
David R. Palmer
Collaborating scientist(s):
Geoff Brundrit, Department of Oceanography, University of Cape Town, South Africa
Leon Krige, Institute for Maritime Technology, Simon's Town, South Africa
Kurt Metzger, Department of Electrical Engineering and Computer Science, University of Michigan
Objective:
The primary goal of the ATOC Program is to measure directly
global ocean temperature trends using innovative underwater
acoustic technologies, based on the fact that the speed of sound
in water is proportional to temperature. The goal of this
particular project is to conduct feasibility studies that will
lead to an appropriate design for the Atlantic component of the
planned ATOC global monitoring network.
Rationale:
Since ocean temperature is a key indicator of global climate
change, accurate temperature measurements, spanning the world's
ocean basins and sampled over a long period, are essential to
complement atmospheric measurements of global climate trends.
The capability to make synoptic temperature estimates derived
directly from acoustic travel time measurements was demonstrated
in the 1991 Heard Island Feasibility Test (Refs. 1-3 below and
sound file) where acoustic signals were transmitted
from a location in the Southern Indian Ocean to 14 receiver stations,
manned by nine international scientific teams, in the Atlantic,
Indian, and Pacific oceans. The test demonstrated that acoustic
signals of moderate intensity can be received over global paths
with sufficient signal to noise ratios to measure propagation
time and spatial variability.
Method:
This effort focuses on the Atlantic Ocean because it is in the
Atlantic that the interaction between the ocean and atmosphere
is strongest and where one is likely to first observe in the
ocean a long term climate trend. The approach involves design
studies for an Atlantic network and sea trials to measure
propagation characteristics between candidate nodes
(source/receiver sites) in the network.
Accomplishment:
Propagation studies were conducted between Cape Town and
Ascension Island during November and December of 1992 (Refs. 5
and 6 below). The primary goal of the studies was to determine
the extent that the acoustic path between Ascension and Cape
Town is blocked by bathymetric features including
the Walvis Ridge, which forms the southern boundary of the Angola Abyssal
Plain, Valdivia Seamount, Bonaparte Seamount, and Grattan
Seamount. These studies demonstrate that one can not
only
find appropriate source-receiver
geometry's for which bathymetric interference can be minimized
but also that the Cape Town site can be picked on the edge of
the continental shelf -- a desirable location for logistical
reasons.
In addition, it was shown that for SOFAR propagation
of incoherent sound over the distance of the experiment (4,300
km), a typical precision in travel time is 0.2 to 0.3 seconds.
In only exceptional, high signal to noise situations can one
expect to be able to measure arrival-time differences on nearby
hydrophones to within 0.1 seconds. (Ref. 6 below)
A feasibility study for a North Atlantic Acoustic Thermometry of
Ocean Climate (ATOC) program has been competed (Ref. 7 below).
The study was requested by the Scientific Committee on Oceanic
Research (SCOR) Working Group 96 (Global Acoustic Monitoring of
the Ocean).
Key reference:
1) D. R. Palmer et al., Reception at Ascension Island, South
Atlantic, of the Transmission from the Heard Island Feasibility
Test, NOAA Technical Memorandum ERL AOML-73 (February 1993)
(available from the first author).
2) D. R. Palmer et al., Reception at Ascension of the Heard
Island Feasibility Test transmission, Journal of the Acoustical
Society of America vol. 96, 2432-2440 (1994).
3) D. R. Palmer, The Ascension Island Listening Station,
Journal of the Acoustical Society of America vol. 90, 2330
(1991) (abstract); also Proceedings of the First International
Meeting on Global Acoustic Monitoring of the Oceans, La Jolla,
1992.
4) D. R. Palmer, Tropical Atlantic Network Design
Considerations, Proceedings of the Second International Meeting
on Global Acoustic Monitoring of the Ocean, Brest, 1993.
5) G. Brundrit, L Krige, D. R. Palmer, J. Penrose, A. Forbes,
and K. Metzger, Acoustic Thermometry of Ocean
Climate-Feasibility Ascension Cape Town, Proceedings of the
Second European Conference on Underwater Acoustics, Copenhagen,
July 1994; also Proceedings of the Second International Meeting
on Global Acoustic Monitoring of the Ocean, Brest, 1993.
6) David Palmer, Leon Krige, Geoff Brundrit, and Kurt Metzger,
ATOC-FACT arrival-time differences, Journal of the Acoustical
Society of America vol. 97, 3265 (1995) (abstract).
7) W. J. Gould, Y. Desaubies, B. M. Howe, D. R. Palmer, F.
Schott, and C. Wunsch, Acoustic Thermometry in the Atlantic,
Proceedings of the Second European Conference on Underwater
Acoustics, Copenhagen, July 1994; also A Report to SCOR WG 96,
Scientific Committee on Oceanic Research, International Council
of Scientific Unions, 1994.
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